Watch the Dallas Symposium LIVE, and fundraiser auction
Ticket proceeds support mindat.org! - click here...
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

(2005) Flow of partially molten crust and origin of detachments during collapse of the Cordilleran Orogen, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 39-64 doi:10.1144/gsl.sp.2005.245.01.03

Advanced
   -   Only viewable:
Reference TypeReport (article/chapter)
TitleFlow of partially molten crust and origin of detachments during collapse of the Cordilleran Orogen
ReportSpecial Publication
Year2005Volume245
PublisherGeological Society of London
DOIdoi:10.1144/gsl.sp.2005.245.01.03Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID432840Long-form Identifiermindat:1:5:432840:1
GUID0
Full Reference(2005) Flow of partially molten crust and origin of detachments during collapse of the Cordilleran Orogen, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 39-64 doi:10.1144/gsl.sp.2005.245.01.03
Plain Text(2005) Flow of partially molten crust and origin of detachments during collapse of the Cordilleran Orogen, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 39-64 doi:10.1144/gsl.sp.2005.245.01.03
InBruhn, David, Burlini, Luigi - Eds. (2005) High-Strain Zones: Structure and Physical Properties. Special Publication Vol. 245. Geological Society of London

See Also

These are possibly similar items as determined by title/reference text matching only.

(2005) Initiation of basement thrust detachments by fault-zone reaction weakening, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 347-372 doi:10.1144/gsl.sp.2005.245.01.17
(2005) High-strain zones: laboratory perspectives on strain softening during ductile deformation, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 1-24 doi:10.1144/gsl.sp.2005.245.01.01
(2005) About this title, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. doi:10.1144/gsl.sp.2005.245.01.23
(2005) The effect of grain size and melt distributions on the rheology of partially molten olivine aggregates, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 291-302 doi:10.1144/gsl.sp.2005.245.01.14
(2005) Rigid polygons in shear, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 421-431 doi:10.1144/gsl.sp.2005.245.01.21
(2005) Shear strain localization from the upper mantle to the middle crust of the Kohistan Arc (Pakistan), in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 25-38 doi:10.1144/gsl.sp.2005.245.01.02
(2005) Electrical conductivity images of active and fossil fault zones, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 165-186 doi:10.1144/gsl.sp.2005.245.01.08
(2005) Experimental deformation of flint in axial compression, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 251-276 doi:10.1144/gsl.sp.2005.245.01.12
(2005) High-strain deformation tests on natural gypsum aggregates in torsion, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 277-290 doi:10.1144/gsl.sp.2005.245.01.13
(2005) Creep constitutive laws for rocks with evolving structure, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 329-346 doi:10.1144/gsl.sp.2005.245.01.16
(2005) Damage and recovery of calcite rocks deformed in the cataclastic regime, in High-Strain Zones: Structure and Physical Properties. Special Publication, 245. Geological Society of London. 203-221 doi:10.1144/gsl.sp.2005.245.01.10
 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are Β© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: August 15, 2025 11:15:16
Go to top of page